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The Upper Tisa Valley. Preparatory proposal for Ramsay

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surrounding plain as an island in which faunas corresponding with 3 fauna-zones<br />

distinct from one another, have survived still in these days.<br />

<strong>The</strong> recent microclimatic and malacological investigations (Sólymos, 1997,<br />

Sólymos-Nagy, 1997) suggest that the microclimate of the hill slopes has direct and<br />

indirect effects on molluscs. Direct effects are linked with the temperature and the<br />

relative humidity of the biotope. <strong>The</strong> interrelation between the air and the plants has an<br />

indirect effect: closed and transitional vegetation can keep an increase in humidity,<br />

which is favourable <strong>for</strong> molluscs. This interrelation is very important because plants as<br />

generative surface generate the microclimate and this microclimate provides many<br />

other living organisms, such as molluscs with proper conditions. It seems to us that<br />

some different microclimatic mosaics and lithobiomes (Huggett, 1995) developed on<br />

the slopes of Kaszony Hill, thus the different ecological habitat loving Mollusc species<br />

(e.g. open or shade loving communities) can live close to each other.<br />

According to the qurtermalacological data (Sümegi-Szabó, 1992) similar<br />

mosaic-like habitat developed on these hill slopes during the Pleistocene when the<br />

“cold stage” taxa and “warm stage” taxa (Willis et al. 1995) could survive some<br />

different climatic changes in small approving environmental pockets (or oasies: Willis<br />

et al. 1998) there<strong>for</strong>e there were highly mixed communities in both flora and fauna.<br />

Thus these hillslopes were favourable places <strong>for</strong> temperate refugial populations, firstly<br />

Carpathian and Middle European <strong>for</strong>est elements.<br />

474<br />

Malakofaunistical evaluation of two floodplain <strong>for</strong>ests<br />

<strong>The</strong> Chilostoma banaticum species, according to our researches live on two<br />

floodplain regions of the Szatmár-Bereg Plain. It was first discovered by Bába (1969)<br />

in the Bagiszeg Forest belonging to a town of Vásárosnamény. Later it was also found<br />

in Szabó-füzes Forest near Tiszabecs (Fintha et al, 1993).<br />

In the course of the biological inventory we collected samples from 8-8<br />

quadrats, and a great amount of material was collected with the bulk method. On the<br />

two territories we found 26 species altogether which is more than 50% of the species<br />

found on the Szatmár-Bereg Plain. <strong>The</strong> common species almost without exception, are<br />

of SE-European, European and Carpathian expansion.<br />

Most of the snails, living only near Bagiszeg, are species existing in European<br />

closed <strong>for</strong>ests. All of the species living only in Tiszabecs are wide-spread holarctic and<br />

palearctic ones which favoure humid, watery biotops independetly from light intensity.<br />

<strong>The</strong> spectacular difference comes from the water-supply of the biotops. <strong>The</strong> odd thing<br />

is that we found twice as many entities in Bagiszeg as in Tiszabecs from the same<br />

amount of quadrats (8-8). This diversity cames from the great density of entities of the<br />

small-sized species, which is due to the luxuriant undergrouth and the thicker <strong>for</strong>est<br />

floor meaning a more favourable biotop <strong>for</strong> them.<br />

According to our research besides Chilostoma banaticum as the dominant<br />

species - we can also find Bradybaena fruticum, Helix pomatia, Cepaea vindobonensis

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